Due to rapid salinity reduction of the influent, the migration and interception of the released clay particles such as illite, kaolinite and chlorite resulted in the permeability change.

 
  • 由于流入液含鹽量的迅速降低,從含水介質(zhì)釋放的黏土顆粒(伊利石、高嶺土和綠泥石)產(chǎn)生運移和截獲,最后導致滲透性的變化。
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